摘要
文章阐述了川北砂岩型铀矿床的地球化学特征。根据能谱测量,用U,Th,K元素的丰度和比值,获得铀富集的有利条件、不利条件。通过伽马能谱法(测U,Th,K)和X射线荧光法(测As,Ba),区分含铀浅色砂岩和不含铀浅色砂岩,区分红色砂岩(红色泥岩)与浅色砂岩,缩小川北砂岩找铀矿的范围。
Expounding geochemical characteristics of sandstone-type uranium deposits in northern Sichuan,this paper demonstrates the favourable and unfavourable conditions for enrichment of uranium on the basis of element abundances and ratios of U,Th and K measured by the gamma-ray spectroscopy surveying. The differences between uranium-bearing and non-uranium sandstones and between red sandstone (claystone) and greenish sandstone can be determined by the gamma-ray spectroscopy (measuring U,Th and K) and XRF analysis (measuring As and Ba). Therefore, the prospecting of the sandstone-type uranium deposits in northern Sichuan can be concentrated in a certain ranse.
出处
《成都理工学院学报》
CAS
CSCD
1994年第2期29-35,共7页
Journal of Chengdu University of Technology
关键词
砂岩
含铀
地球化学
矿化
铀矿床
northern Sichuan
sandstone-type uranium doposit
ore-bearing host rock
elemental geochemistry
identification of metullogeny